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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F06%3A00017189%21RIV10-MSM-14310___
rdf:type
n12:Vysledek skos:Concept
dcterms:description
The early Variscan phase of the evolution of Brunovistulian terrane was characterized by the formation of Devonian extensional basins and WPA volcanic activity. The compressive phase is recorded in synorogenic flysch sedimentation, which shows a distinct polarity. The oldest flysch (Protivanov and Andelska Hora Fm.) contains clastic micas from early Paleozoic crystalline rocks that are assumed to be derived either from an active Brunovistulian margin, now covered by the Lugodanubian nappes, or from the terranes of Armorican affinity. At the beginning of the Namurian the development of the Moravo-Silesian late Paleozoic basin was terminated by coal-bearing paralic and limnic sediments. The progressive Carboniferous stacking of nappes and their impingement on the Laurussian foreland led to crustal thickening and shortening. The Devonian preorogenic and Carboniferous synorogenic sedimentation bears close similarity to the Rhenohercynian Zone of Germany. The early Variscan phase of the evolution of Brunovistulian terrane was characterized by the formation of Devonian extensional basins and WPA volcanic activity. The compressive phase is recorded in synorogenic flysch sedimentation, which shows a distinct polarity. The oldest flysch (Protivanov and Andelska Hora Fm.) contains clastic micas from early Paleozoic crystalline rocks that are assumed to be derived either from an active Brunovistulian margin, now covered by the Lugodanubian nappes, or from the terranes of Armorican affinity. At the beginning of the Namurian the development of the Moravo-Silesian late Paleozoic basin was terminated by coal-bearing paralic and limnic sediments. The progressive Carboniferous stacking of nappes and their impingement on the Laurussian foreland led to crustal thickening and shortening. The Devonian preorogenic and Carboniferous synorogenic sedimentation bears close similarity to the Rhenohercynian Zone of Germany.
dcterms:title
Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane, Czech Republic Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane, Czech Republic
skos:prefLabel
Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane, Czech Republic Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane, Czech Republic
skos:notation
RIV/00216224:14310/06:00017189!RIV10-MSM-14310___
n3:aktivita
n17:Z
n3:aktivity
Z(MSM0021622412)
n3:dodaniDat
n13:2010
n3:domaciTvurceVysledku
n10:6213405 n10:6504507 n10:1283987 n10:7162286 n10:3032744
n3:druhVysledku
n5:D
n3:duvernostUdaju
n16:S
n3:entitaPredkladatele
n18:predkladatel
n3:idSjednocenehoVysledku
503213
n3:idVysledku
RIV/00216224:14310/06:00017189
n3:jazykVysledku
n9:eng
n3:klicovaSlova
stratigraphy; Brunovistulian terrane; Rhenohercynian zone; Variscan orogeny; tectonostratigraphy; Devonian; Carboniferous
n3:klicoveSlovo
n11:Rhenohercynian%20zone n11:Devonian n11:tectonostratigraphy n11:stratigraphy n11:Carboniferous n11:Variscan%20orogeny n11:Brunovistulian%20terrane
n3:kontrolniKodProRIV
[1274B933BD4C]
n3:mistoKonaniAkce
Köln
n3:mistoVydani
Köln
n3:nazevZdroje
Carboniferous Conference Cologne. From Platform to Basin, Sept. 4-10 2006. Kölner Forum für Geologie und Paläontologie, 15.
n3:obor
n15:DB
n3:pocetDomacichTvurcuVysledku
5
n3:pocetTvurcuVysledku
5
n3:rokUplatneniVysledku
n13:2006
n3:tvurceVysledku
Bábek, Ondřej Kalvoda, Jiří Leichmann, Jaromír Melichar, Rostislav Špaček, Petr
n3:typAkce
n4:WRD
n3:zahajeniAkce
2006-09-04+02:00
n3:zamer
n7:MSM0021622412
s:numberOfPages
2
n19:hasPublisher
Institut für Geologie und Mineralogie der Universität zu Köln
n6:isbn
3-934027-18-0
n21:organizacniJednotka
14310